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Plate Tectonics

Published on Nov 20, 2015

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PRESENTATION OUTLINE

PLATE TECTONICS

Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core.

SLAB PULL

The pull of gravity on a plate that is being subducted

CONVECTION CURRENTS

The transfer of heat by the mass movement of heated particles into an area of cooler fluid

SUBDUCTION

The process when one tectonic plate moves underneath another

DIVERGENT PLATE BOUNDARY

As the plate move apart magma comes up and cools make more floor

RIFT VALLEY

DIVERGENT LANDFORM (LAND)

MID OCEAN RIDGE

DIVERGENT LANDFORM (SEA)

CONVERGENT PLATE BOUNDARY

Is When Tectonic plates or fragments of the lithosphere move toward one another and collide.

HIMALYAN MOUNTAINS

CONTINENTAL V.S CONTINENTAL

CHILE PERU SEA TRENCH WITH ANDES MTS. VOLCANIC ARC

CONTINENTAL V.S OCEAN

MARINA TRENCH AND JAPAN TRENCH ISLAND ARC

Caused by ocean vs ocean

SUBDUCTION ZONE

Collision between two of the planet's tectonic plates and one plate goes under another

DEEP OCEAN TRENCH

Oceanic crust is formed at an oceanic ridge, while the lithosphere is subducted back into the asthenosphere at trenches.

DEEP OCEAN TRENCH EXAMPLE

Marianas Trench

TRANSFORM PLATE BOUNDARY

San Andreas fault, earthquakes, no crust is destroyed or created and it slides horizontally